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Uranium-bearing veins in the United States are principally fissure-filling deposits in faults, joints, or fracture zones that have resulted from compressive, tensile, or torsional stresses. The individual ore bodies within vein deposits are tabular sheetlike masses or ore shoots along veins, irregular stockworks along fault zones, or pipelike masses either in fault intersections or in blocks of broken ground. Many veins consist of gouge or breccia containing uranium minerals. Rocks adjacent to faults, joints, or fault zones may also contain uranium if they are porous or reactive, or if they are broken. Most uranium-bearing vein districts in the United States are in structural environments in which subsidiary intermediateto small-scale faults and folds are related spatially to largeto intermediate-scale folds, anticlinal uplifts, crystalline-rock masses, or faults. Deposition of uranium commonly occurs late in the structural history of a district.

Structural control of uranium-bearing vein deposits and districts in the conterminous United States